The amount of radiation depends upon the position of the sun in the sky as the lower the position the more energy is absorbed by the earth's atmosphere. This gives rise to the observed temperature variations during the day, between summer and winter and between the north and south of any country. The annual mean solar radiation for the UK is shown left.
Whilst on a sunny day, solar radiation can be directly received, on a cloudy day less radiation is received because it is scattered by the water droplets on the clouds. Typical values are shown below. |